首页> 外文会议>Conference on earth observation for land-atmosphere interaction science >SURFACE-ATMOSPHERE INTERACTIONS DURING A POLYNYA EVENT AT TERRA NOVA BAY (ANTARCTICA)
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SURFACE-ATMOSPHERE INTERACTIONS DURING A POLYNYA EVENT AT TERRA NOVA BAY (ANTARCTICA)

机译:Terra Nova Bay(南极洲)的Polynya活动期间的表面大气互动

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Numerical three-dimensional weather simulations, satellite imagery and automatic weather station (AWS) data are used to study a real event of coastal polynya at Terra Nova Bay (TNB), Antarctica. The event, detected with satellite images, occurred in the period 12–17 July 2006. The atmospheric simulations are performed by the limited area Eta Model. Passive microwave satellite images, which are not affected by cloud cover, are used to evaluate the daily polynya size, while thermal infrared satellite images are only used to follow cloud dynamics. The synoptic and sub-synoptic fields are very well represented by the model results when they are compared with AVHRR imagery. Comparisons between simulated data and wind measurements by Manuela AWS are presented as well. The results are considered satisfactory. Simulation results show the striking relationship of surface winds and temperatures with the development of the polynya as inferred by satellite images
机译:数值三维天气模拟,卫星图像和自动气象站(AWS)数据用于研究Terra Nova Bay(TNB),南极洲的沿海Polynya的真正活动。 通过卫星图像检测到的事件发生在2006年7月12日至77日。大气模拟由有限的ETA模型进行。 无源微波卫星图像不受云覆盖的影响,用于评估每日多玉田尺寸,而热红外卫星图像仅用于遵循云动态。 当与AVHRR Imagerery进行比较时,模型结果非常良好地表示天气和子概要字段。 Smanela AWS的模拟数据和风测量之间的比较也是如此。 结果被认为是令人满意的。 仿真结果表明,随着卫星图像推断的,仿真和温度随着卫星图像推断的醒目关系

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